C $Header: /home/ubuntu/mnt/e9_copy/MITgcm/pkg/seaice/seaice_init_fixed.F,v 1.14 2012/02/09 03:42:32 gforget Exp $ C $Name: $ #include "SEAICE_OPTIONS.h" CStartOfInterface SUBROUTINE SEAICE_INIT_FIXED( myThid ) C *==========================================================* C | SUBROUTINE SEAICE_INIT_FIXED C | o Initialization of sea ice model. C *==========================================================* C *==========================================================* IMPLICIT NONE C === Global variables === #include "SIZE.h" #include "EEPARAMS.h" #include "PARAMS.h" #include "GRID.h" #include "FFIELDS.h" #include "SEAICE_PARAMS.h" #include "SEAICE.h" C === Routine arguments === C myThid - Thread no. that called this routine. INTEGER myThid CEndOfInterface C === Local variables === C i,j,k,bi,bj - Loop counters INTEGER i, j, bi, bj INTEGER kSurface #ifndef SEAICE_CGRID _RS mask_uice #endif #ifdef SHORTWAVE_HEATING cif Helper variable for determining the fraction of sw radiation cif penetrating the model shallowest layer _RL dummyTime _RL swfracba(2) _RL tmpFac #endif /* SHORTWAVE_HEATING */ IF ( buoyancyRelation .EQ. 'OCEANICP' ) THEN kSurface = Nr ELSE kSurface = 1 ENDIF C Initialize MNC variable information for SEAICE IF ( useMNC .AND. & (seaice_tave_mnc.OR.seaice_dump_mnc.OR.SEAICE_mon_mnc) & ) THEN CALL SEAICE_MNC_INIT( myThid ) ENDIF _BEGIN_MASTER(myThid) #ifdef SHORTWAVE_HEATING tmpFac = -1.0 dummyTime = 1.0 swfracba(1) = ABS(rF(1)) swfracba(2) = ABS(rF(2)) CALL SWFRAC( I 2, tmpFac, U swfracba, I dummyTime, 0, myThid ) SWFracB = swfracba(2) #else /* SHORTWAVE_HEATING */ SWFracB = 0. _d 0 #endif /* SHORTWAVE_HEATING */ _END_MASTER(myThid) C-- efficiency of ocean-ice turbulent flux ... if (SEAICEturbFluxFormula.EQ.1) then c ... can be specified as fractions between 0 and 1 IF ( SEAICE_availHeatFrac .EQ. UNSET_RL ) & SEAICE_availHeatFrac = ONE IF ( SEAICE_availHeatFracFrz .EQ. UNSET_RL ) & SEAICE_availHeatFracFrz = SEAICE_availHeatFrac elseif (SEAICEturbFluxFormula.EQ.2) then c ... can be specified as time scales (>SEAICE_deltaTtherm) IF ( SEAICE_gamma_t .EQ. UNSET_RL ) & SEAICE_gamma_t=SEAICE_deltaTtherm IF ( SEAICE_gamma_t_frz .EQ. UNSET_RL ) & SEAICE_gamma_t_frz=SEAICE_gamma_t IF ( SEAICE_gamma_t .LE. SEAICE_deltaTtherm ) THEN SEAICE_availHeatFracFrz = 1. _d 0 ELSE SEAICE_availHeatFrac = SEAICE_deltaTtherm/SEAICE_gamma_t ENDIF IF ( SEAICE_gamma_t_frz .LE. SEAICE_deltaTtherm ) THEN SEAICE_availHeatFracFrz = 1. _d 0 ELSE SEAICE_availHeatFracFrz = & SEAICE_deltaTtherm/SEAICE_gamma_t_frz ENDIF elseif ( (SEAICEturbFluxFormula.EQ.3).OR. & (SEAICEturbFluxFormula.EQ.4) ) then c ... is hard-coded (after McPhee) SEAICE_availHeatFrac= MCPHEE_TAPER_FAC * STANTON_NUMBER * & USTAR_BASE / dRf(kSurface) * SEAICE_deltaTtherm SEAICE_availHeatFracFrz=ZERO endif C-- convert SEAICE_doOpenWaterGrowth/Melt logical switch to numerical facOpenGrow/Melt facOpenGrow=0. _d 0 facOpenMelt=0. _d 0 if (SEAICE_doOpenWaterGrowth) facOpenGrow=1. _d 0 if (SEAICE_doOpenWaterMelt) facOpenMelt=1. _d 0 C-- Initialize grid info DO bj=myByLo(myThid),myByHi(myThid) DO bi=myBxLo(myThid),myBxHi(myThid) DO j=1-OLy,sNy+OLy DO i=1-OLx,sNx+OLx HEFFM(i,j,bi,bj) = 0. _d 0 ENDDO ENDDO DO j=1-OLy,sNy+OLy DO i=1-OLx,sNx+OLx HEFFM(i,j,bi,bj)= 1. _d 0 IF (_hFacC(i,j,kSurface,bi,bj).eq.0.) & HEFFM(i,j,bi,bj)= 0. _d 0 ENDDO ENDDO #ifndef SEAICE_CGRID DO j=1-OLy+1,sNy+OLy DO i=1-OLx+1,sNx+OLx UVM(i,j,bi,bj)=0. _d 0 mask_uice=HEFFM(i,j, bi,bj)+HEFFM(i-1,j-1,bi,bj) & +HEFFM(i,j-1,bi,bj)+HEFFM(i-1,j, bi,bj) IF(mask_uice.GT.3.5 _d 0) UVM(i,j,bi,bj)=1. _d 0 ENDDO ENDDO #endif /* SEAICE_CGRID */ ENDDO ENDDO C coefficients for metric terms DO bj=myByLo(myThid),myByHi(myThid) DO bi=myBxLo(myThid),myBxHi(myThid) #ifdef SEAICE_CGRID DO j=1-OLy,sNy+OLy DO i=1-OLx,sNx+OLx k1AtC(I,J,bi,bj) = 0.0 _d 0 k1AtZ(I,J,bi,bj) = 0.0 _d 0 k2AtC(I,J,bi,bj) = 0.0 _d 0 k2AtZ(I,J,bi,bj) = 0.0 _d 0 ENDDO ENDDO IF ( usingSphericalPolarGrid .AND. SEAICEuseMetricTerms ) THEN C This is the only case where tan(phi) is not zero. In this case C C and U points, and Z and V points have the same phi, so that we C only need a copy here. Do not use tan(YC) and tan(YG), because these C can be the geographical coordinates and not the correct grid C coordinates when the grid is rotated (phi/theta/psiEuler .NE. 0) DO j=1-OLy,sNy+OLy DO i=1-OLx,sNx+OLx k2AtC(I,J,bi,bj) = - _tanPhiAtU(I,J,bi,bj)*recip_rSphere k2AtZ(I,J,bi,bj) = - _tanPhiAtV(I,J,bi,bj)*recip_rSphere ENDDO ENDDO ELSEIF ( usingCurvilinearGrid .AND. SEAICEuseMetricTerms ) THEN C compute metric term coefficients from finite difference approximation DO j=1-OLy,sNy+OLy DO i=1-OLx,sNx+OLx-1 k1AtC(I,J,bi,bj) = _recip_dyF(I,J,bi,bj) & * ( _dyG(I+1,J,bi,bj) - _dyG(I,J,bi,bj) ) & * _recip_dxF(I,J,bi,bj) ENDDO ENDDO DO j=1-OLy,sNy+OLy DO i=1-OLx+1,sNx+OLx k1AtZ(I,J,bi,bj) = _recip_dyU(I,J,bi,bj) & * ( _dyC(I,J,bi,bj) - _dyC(I-1,J,bi,bj) ) & * _recip_dxV(I,J,bi,bj) ENDDO ENDDO DO j=1-OLy,sNy+OLy-1 DO i=1-OLx,sNx+OLx k2AtC(I,J,bi,bj) = _recip_dxF(I,J,bi,bj) & * ( _dxG(I,J+1,bi,bj) - _dxG(I,J,bi,bj) ) & * _recip_dyF(I,J,bi,bj) ENDDO ENDDO DO j=1-OLy+1,sNy+OLy DO i=1-OLx,sNx+OLx k2AtZ(I,J,bi,bj) = _recip_dxV(I,J,bi,bj) & * ( _dxC(I,J,bi,bj) - _dxC(I,J-1,bi,bj) ) & * _recip_dyU(I,J,bi,bj) ENDDO ENDDO ENDIF #else /* not SEAICE_CGRID */ DO j=1-OLy,sNy+OLy DO i=1-OLx,sNx+OLx k1AtC(I,J,bi,bj) = 0.0 _d 0 k1AtU(I,J,bi,bj) = 0.0 _d 0 k1AtV(I,J,bi,bj) = 0.0 _d 0 k2AtC(I,J,bi,bj) = 0.0 _d 0 k2AtU(I,J,bi,bj) = 0.0 _d 0 k2AtV(I,J,bi,bj) = 0.0 _d 0 ENDDO ENDDO IF ( usingSphericalPolarGrid .AND. SEAICEuseMetricTerms ) THEN C This is the only case where tan(phi) is not zero. In this case C C and U points, and Z and V points have the same phi, so that we C only need a copy here. Do not use tan(YC) and tan(YG), because these C can be the geographical coordinates and not the correct grid C coordinates when the grid is rotated (phi/theta/psiEuler .NE. 0) DO j=1-OLy,sNy+OLy DO i=1-OLx,sNx+OLx k2AtC(I,J,bi,bj) = - _tanPhiAtU(I,J,bi,bj)*recip_rSphere k2AtU(I,J,bi,bj) = - _tanPhiAtU(I,J,bi,bj)*recip_rSphere k2AtV(I,J,bi,bj) = - _tanPhiAtV(I,J,bi,bj)*recip_rSphere ENDDO ENDDO ELSEIF ( usingCurvilinearGrid .AND. SEAICEuseMetricTerms ) THEN C compute metric term coefficients from finite difference approximation DO j=1-OLy,sNy+OLy DO i=1-OLx,sNx+OLx-1 k1AtC(I,J,bi,bj) = _recip_dyF(I,J,bi,bj) & * ( _dyG(I+1,J,bi,bj) - _dyG(I,J,bi,bj) ) & * _recip_dxF(I,J,bi,bj) ENDDO ENDDO DO j=1-OLy,sNy+OLy DO i=1-OLx+1,sNx+OLx k1AtU(I,J,bi,bj) = _recip_dyG(I,J,bi,bj) & * ( _dyF(I,J,bi,bj) - _dyF(I-1,J,bi,bj) ) & * _recip_dxC(I,J,bi,bj) ENDDO ENDDO DO j=1-OLy,sNy+OLy DO i=1-OLx,sNx+OLx-1 k1AtV(I,J,bi,bj) = _recip_dyC(I,J,bi,bj) & * ( _dyU(I+1,J,bi,bj) - _dyU(I,J,bi,bj) ) & * _recip_dxG(I,J,bi,bj) ENDDO ENDDO DO j=1-OLy,sNy+OLy-1 DO i=1-OLx,sNx+OLx k2AtC(I,J,bi,bj) = _recip_dxF(I,J,bi,bj) & * ( _dxG(I,J+1,bi,bj) - _dxG(I,J,bi,bj) ) & * _recip_dyF(I,J,bi,bj) ENDDO ENDDO DO j=1-OLy,sNy+OLy-1 DO i=1-OLx,sNx+OLx k2AtU(I,J,bi,bj) = _recip_dxC(I,J,bi,bj) & * ( _dxV(I,J+1,bi,bj) - _dxV(I,J,bi,bj) ) & * _recip_dyG(I,J,bi,bj) ENDDO ENDDO DO j=1-OLy+1,sNy+OLy DO i=1-OLx,sNx+OLx k2AtV(I,J,bi,bj) = _recip_dxG(I,J,bi,bj) & * ( _dxF(I,J,bi,bj) - _dxF(I,J-1,bi,bj) ) & * _recip_dyC(I,J,bi,bj) ENDDO ENDDO ENDIF #endif /* not SEAICE_CGRID */ ENDDO ENDDO #ifndef SEAICE_CGRID C-- Choose a proxy level for geostrophic velocity, DO bj=myByLo(myThid),myByHi(myThid) DO bi=myBxLo(myThid),myBxHi(myThid) DO j=1-OLy,sNy+OLy DO i=1-OLx,sNx+OLx KGEO(i,j,bi,bj) = 0 ENDDO ENDDO DO j=1-OLy,sNy+OLy DO i=1-OLx,sNx+OLx #ifdef SEAICE_BICE_STRESS KGEO(i,j,bi,bj) = 1 #else /* SEAICE_BICE_STRESS */ IF (klowc(i,j,bi,bj) .LT. 2) THEN KGEO(i,j,bi,bj) = 1 ELSE KGEO(i,j,bi,bj) = 2 DO WHILE ( abs(rC(KGEO(i,j,bi,bj))) .LT. 50.0 _d 0 .AND. & KGEO(i,j,bi,bj) .LT. (klowc(i,j,bi,bj)-1) ) KGEO(i,j,bi,bj) = KGEO(i,j,bi,bj) + 1 ENDDO ENDIF #endif /* SEAICE_BICE_STRESS */ ENDDO ENDDO ENDDO ENDDO #endif /* SEAICE_CGRID */ #ifdef ALLOW_DIAGNOSTICS IF ( useDiagnostics ) THEN CALL SEAICE_DIAGNOSTICS_INIT( myThid ) ENDIF #endif C-- Summarise pkg/seaice configuration CALL SEAICE_SUMMARY( myThid ) RETURN END